地理学报 ›› 2017, Vol. 72 ›› Issue (11): 2018-2031.doi: 10.11821/dlxb201711008
所属专题: 气候变化与地表过程
乔琨1,2,3(), 朱文泉1,2, 胡德勇3(
), 郝明4, 陈姗姗3, 曹诗颂3
收稿日期:
2017-03-29
修回日期:
2017-07-10
出版日期:
2017-11-20
发布日期:
2017-11-16
作者简介:
作者简介:乔琨(1989-), 女, 河北人, 博士, 研究方向为资源环境遥感、植被遥感。E-mail:
基金资助:
Kun QIAO1,2,3(), Wenquan ZHU1,2, Deyong HU3(
), Ming HAO4, Shanshan CHEN3, Shisong CAO3
Received:
2017-03-29
Revised:
2017-07-10
Online:
2017-11-20
Published:
2017-11-16
Supported by:
摘要:
目前有关北京市不透水地表的相关研究多数是从整体层面开展,忽略了其内部功能区的作用及差异。运用分类回归树(CART)及系列变化检测模型得到北京市1991年、2001年、2011年和2015年四期不透水地表分布,并运用标准差椭圆、洛伦兹曲线、贡献指数及景观格局理论对各功能区不透水地表的时空变化进行分析。结果显示:1991-2015年北京市不透水地表的总面积增加了约144.18%,分布的主导方向由早期的东北—西南趋向于当前的正北—正南。各功能区间不透水地表的空间分布异质性逐渐减弱,但贡献指数值存在很大差异:功能拓展区的贡献指数最高,其四年中的最低值(1.79)高于其他功能区四年最高值,是北京市不透水地表增长最主要的贡献区;功能核心区的蔓延度指数值最高,约为其他功能区的2倍,为不透水地表的优势聚集区;发展新区的贡献值由负值变为正值并成倍增长,成为北京市不透水地表增长的主要源区;生态涵养发展区的贡献指数始终为负,并逐年减小。不同类型不透水地表的景观指数和质心偏移均存在差异,高盖度不透水地表的形状指数和斑块密度值最小,分布最为集中,对生态环境影响较大,北京市在未来发展过程中应合理规划控制其空间格局及增长模式,尽量减缓其增长速度及团聚程度。
乔琨, 朱文泉, 胡德勇, 郝明, 陈姗姗, 曹诗颂. 北京市不同功能区不透水地表时空变化差异[J]. 地理学报, 2017, 72(11): 2018-2031.
Kun QIAO, Wenquan ZHU, Deyong HU, Ming HAO, Shanshan CHEN, Shisong CAO. Examining the distribution and dynamics of impervious surface in different functional zones of Beijing[J]. Acta Geographica Sinica, 2017, 72(11): 2018-2031.
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